首页> 外文期刊>Petroleum science >The coupling of dynamics and permeability in the hydrocarbon accumulation period controls the oil-bearing potential of low permeability reservoirs: a case study of the low permeability turbidite reservoirs in the middle part of the third member of Shahejie Formation in Dongying Sag
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The coupling of dynamics and permeability in the hydrocarbon accumulation period controls the oil-bearing potential of low permeability reservoirs: a case study of the low permeability turbidite reservoirs in the middle part of the third member of Shahejie Formation in Dongying Sag

机译:油气成藏期动力学与渗透率的耦合控制了低渗透油藏的含油潜力:以东营凹陷沙河街组三段中段低渗透浊积岩油藏为例。

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The relationships between permeability and dynamics in hydrocarbon accumulation determine oil-bearing potential (the potential oil charge) of low permeability reservoirs. The evolution of porosity and permeability of low permeability turbidite reservoirs of the middle part of the third member of the Shahejie Formation in the Dongying Sag has been investigated by detailed core descriptions, thin section analyses, fluid inclusion analyses, carbon and oxygen isotope analyses, mercury injection, porosity and permeability testing, and basin modeling. The cutoff values for the permeability of the reservoirs in the accumulation period were calculated after detailing the accumulation dynamics and reservoir pore structures, then the distribution pattern of the oil-bearing potential of reservoirs controlled by the matching relationship between dynamics and permeability during the accumulation period were summarized. On the basis of the observed diagenetic features and with regard to the paragenetic sequences, the reservoirs can be subdivided into four types of diagenetic facies. The reservoirs experienced two periods of hydrocarbon accumulation. In the early accumulation period, the reservoirs except for diagenetic facies A had middle to high permeability ranging from 10?×?10~(?3)?μm~(2) to 4207?×?10~(?3?)?μm~(2). In the later accumulation period, the reservoirs except for diagenetic facies C had low permeability ranging from 0.015?×?10~(?3)?μm~(2) to 62?×?10~(?3)?μm~(2). In the early accumulation period, the fluid pressure increased by the hydrocarbon generation was 1.4–11.3?MPa with an average value of 5.1?MPa, and a surplus pressure of 1.8–12.6?MPa with an average value of 6.3?MPa. In the later accumulation period, the fluid pressure increased by the hydrocarbon generation process was 0.7–12.7?MPa with an average value of 5.36?MPa and a surplus pressure of 1.3–16.2?MPa with an average value of 6.5?MPa. Even though different types of reservoirs exist, all can form hydrocarbon accumulations in the early accumulation period. Such types of reservoirs can form hydrocarbon accumulation with high accumulation dynamics; however, reservoirs with diagenetic facies A and diagenetic facies B do not develop accumulation conditions with low accumulation dynamics in the late accumulation period for very low permeability. At more than 3000?m burial depth, a larger proportion of turbidite reservoirs are oil charged due to the proximity to the source rock. Also at these depths, lenticular sand bodies can accumulate hydrocarbons. At shallower depths, only the reservoirs with oil-source fault development can accumulate hydrocarbons. For flat surfaces, hydrocarbons have always been accumulated in the reservoirs around the oil-source faults and areas near the center of subsags with high accumulation dynamics.
机译:渗透率与油气成藏动力学之间的关系决定了低渗透率油藏的含油潜力(潜在的装油量)。通过详细的岩心描述,薄片分析,流体包裹体分析,碳氧同位素分析,汞分析,研究了东营凹陷沙河街组第三段中段低渗浊度浊积岩储层的孔隙度和渗透率演化。注入,孔隙度和渗透率测试以及盆地建模。在详细描述了成藏动态和储层孔隙结构后,计算了成藏期储层渗透率的临界值,然后通过成藏期动力学与渗透率的匹配关系控制了储层含油势的分布规律。总结。根据观察到的成岩特征,并根据共生序列,可将储层划分为四种成岩相。这些油藏经历了两次油气成藏期。在成藏初期,除成岩相A外,其他储集层的中高渗透率范围从10?×?10〜(?3)?μm〜(2)到4207?×?10〜(?3?)?μm。 〜(2)。在成藏后期,除成岩相C外,储层渗透率低,范围为0.015××10〜(?3)?μm〜(2)至62××10〜(?3)?μm〜(2)。 )。在蓄积初期,因生烃而增加的流体压力为1.4-11.3?MPa,平均值为5.1?MPa,过剩压力为1.8-12.6?MPa,平均值为6.3?MPa。在随后的成藏期,烃生过程增加的流体压力为0.7-12.7?MPa,平均值为5.36?MPa,过剩压力为1.3-16.2?MPa,平均值为6.5?MPa。即使存在不同类型的油藏,所有油藏都可以在成藏早期形成油气成藏。这种类型的储层可以形成具有高聚集动力的油气成藏。然而,具有成岩相A和成岩相B的储层在晚期成藏期并没有形成具有低成藏动态的成藏条件,因此渗透率非常低。在埋藏深度超过3000?m时,由于靠近烃源岩,所以浊积岩储层中的油充填比例更高。同样在这些深度,柱状砂体会积聚碳氢化合物。在较浅的深度,只有具有油源断层发育的油藏才能聚集碳氢化合物。对于平坦的表面,碳氢化合物总是聚集在油源断层周围以及下陷中心附近区域的储层中,具有很高的聚集动态。

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